India–Asia convergence driven by the subduction of the Greater Indian continent
Author:
Publisher
Springer Science and Business Media LLC
Subject
General Earth and Planetary Sciences
Link
http://www.nature.com/articles/ngeo725.pdf
Reference30 articles.
1. Patriat, P. & Achache, J. India–Eurasia collision chronology has implications for crustal shortening and driving mechanism of plates. Nature 311, 615–621 (1984).
2. DeCelles, P. G. et al. Stratigraphy, structure, and tectonic evolution of the Himalayan fold-thrust belt in western Nepal. Tectonics 20, 487–509 (2001).
3. Guillot, S. et al. Reconstructing the total shortening history of the NW Himalaya. Geochem. Geophys. Geosyst. 4, 1064 (2003).
4. Ni, J. & Barazangi, M. Seismotectonics of the Himalayan collision zone: Geometry of the underthrusting Indian plate beneath the Himalaya. J. Geophys. Res. 89, 1147–1164 (1984).
5. Powell, C. M. A. & Conaghan, P. J. Plate Tectonics and Himalayas. Earth Planet. Sci. Lett. 20, 1–12 (1973).
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